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/lp/de-gruyter/spatial-diversity-of-gully-density-of-the-lublin-upland-and-roztocze-zIHGoNSlfj
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- Publisher
- de Gruyter
- Copyright
- Copyright © 2012 by the
- ISSN
- 0137-1983
- eISSN
- 2083-3601
- DOI
- 10.2478/v10066-012-0002-y
- Publisher site
- See Article on Publisher Site
Abstract
are concentrated on gullies occur only sporadically and only in the north; in the South Baltic and East differences between gullies and river valleys include absence of a permanent river- a narrow bottom, landforms developing as a result of periodic runoff in episodic river-beds from - The issue of the distribution and density of the gully systems and their devel- h of the young erosion dissections on the hexagon gully density and indicated the relationship between gully distribution and diverse all forms of land - which addresses the issue of the distribution of these landforms and the problem the 20th for the geomorphological regions were calculated using a digitalized geomorpho2 The analysis of the topographic factors of gully distribution was performed using lowed mapping the The study material allowed a detailed analysis of the distribution of gullies 2 that the gully landforms are concentrated in compact distribution of gullies shows a clear correlation with the morphometric features The Goraj Roztocze region has been reported to be the most strongly dis2 2 2 is chara The gully densities in the other geomorphological regions do not exceed d gullies oc- regions are rather unequally distributed; they occur both within geomorphologi- leogeographic factors as well as the high relative altitude values determine the this area is attributed to intensive agricultural management and consequent defor- a region that covers the left side of the Bystra River 35 tem of gullies that developed on the right slope of the Bystra River valley below Dobre by is a gully region in the central part of the left slope of the is a region located on a fragment of the left slope of the cenrain resulted in revival of large-scale erosion activity in the gullies th a region comprising gullies in the escarpment zone of - The upper sections of the catchment of the Sanna and Branew valleys are charcurrent raising the region covers the upper part of the Por River catchment northern slope of Roztocze in this fragment is dissected by a system of dry valleys that are oblique in relation to the main escarpment dislocation formed in the loess cover in the inner ridge of the loess patch and substantial denivelations asareas by gulli horst located between the tectonic grabens of the Gorajec River valley and the ment are typical branching escarpment landforms dissecting the steep northern whose slopes are dissected by an extremely dense system of gullies; these someexhibits a particularly distinct impact of the primary subloessial relief determined occur in the watershed zone descending onto the slopes of the valleys character- Gap of the Middle Vistula Chodel Basin western part eastern part in the Bystra River catchment Goraj Roztocze Szczebrzeszyn Roztocze in the Gorajec River catchment in the Por River catchment Rawa Roztocze Sitaniec Szewnia Niemienice Total Total length of the gullies 644.68 (5.64%) gullies In the analysis of gully distribution using maps of relative heights and loess - nystaw with denivelations exceeding even 90 m is dissected by only few gul- a higher gully density can be found in regions that exhibit a distinct tendency to nessed considerable changes in the land management and land ownership struc- advantage of the gully systems and develop new tourism products based on the -
Journal
Annales UMCS, Geographia, Geologia, Mineralogia et Petrographia – de Gruyter
Published: Jan 1, 2012